Coral reef productivity depends on fast nutrient cycling, mediated largely by enzymatic breakdown of organic matter. Alkaline phosphatases hydrolyse phosphomonoesters and are one of the key enzymes involved in marine phosphorus cycling. They are expressed by a plethora of marine organisms including both planktonic microbes and metazoans such as corals, often in response to phosphate limitation, and are potentially important for coral P nutrition and reef biogeochemical cycling. However, most alkaline phosphatase activity (APA) data are from open-ocean environments, and the rates and drivers of APA in coastal waters are not well understood. Here, we measured APA both in the water column and associated with three coral species at reefs in Singapore, where the monsoonal ocean current reversal creates strong seasonal changes in dissolved nutrient availability. Water column APA was consistently high, averaging 9 ± 10 nmol l-1 h-1, but was not correlated with dissolved phosphate or other biogeochemical parameters. Experimental phosphate addition did not reduce seawater APA but addition of labile organic carbon did increase seawater APA, indicating that the increase in APA was driven by heterotrophic activity rather than phosphate stress. Coral APA ranged from 12–163 µmol m-2 h-1 depending on species and was equivalent to the APA in several meters of overlying water. While most coral APA was associated with the coral holobiont rather than the coral mucus, corals released 12 – 55 µmol h-1 per m2 of mucus-associated APA into the water column, which is potentially significant for water column DOP cycling.